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INTEGRATED PETROPHYSICAL FORMATION EVALUATION USING CAPTURE SPECTROSCOPY AND NMR ON AN EXPLORATION WELL, SOUTH SUMATRA

机译:南苏门答腊一口勘探井的捕获光谱和核磁共振综合岩石物理形成评价

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This paper presents an integrated petrophysical formation evolution on two complicated geology settings penetrated by an exploration well in South Sumatra region. The rich information from the capture spectroscopy and nuclear magnetic resonance provides tremendous applications on fluid typing on the low resistivity contrast sandstones in a fresh formation water environment; and the lithology identification plus other reservoir properties characterization on an unconventional reservoir. The interpretation guided the selection of test candidates and has been confirmed by the test results.rnThe first formation is a clastic sequence where fluid typing was the main challenge. On conventional logs most of the sands have similar petrophysical characters, in terms of the resistivity reading, lack of Density-Neutron cross over, etc. In addition, a dubious clay volume derived from gamma ray and fresh formation water made the interpretation even more challenging.rnIn view of these difficulties, The Company decided to acquire capture spectroscopy and NMR logs in order to reach a solid conclusion for the first exploration well in this structure. All hydrocarbon-bearing zones were clearly identified. The sedimentary sequence for the main gas-bearing sand was clearly revealed by the spectroscopy-NMR combination; for another zone, the spectroscopy log showed a much lower clay volume compared to the traditional GR estimation, and the Density-NMR combination revealed this zone to be gas bearing, even though there was no Density-Neutron cross-over. A gas cap was identified on therntop of massive water-bearing sand, raising expectation that more gas can be found higher in the structure for the same sand.rnAt the bottom of the same well, a very radioactive massive formation was discovered, the natural gamma ray spectrometry showed that both thorium and potassium readings are very high; neutron and density logs cannot provide conclusive lithology and porosity as well. Capture spectroscopy identified one clean sand at the top of the formation. The permeability from NMR is also high. Very long T2 relaxation times are suggesting that there is big potential of existing very light oil.rnThe detailed mineralogical information derived from the comprehensive measurements of gamma ray capture spectroscopy and NMR implies that the sedimentary environment for this formation is most probably an alluvial deposition and the source rock is weathered granite. This log-based conclusion helped in calibrating the existing reservoir model.
机译:本文介绍了南苏门答腊地区一口探井穿透的两个复杂地质环境下的综合岩石物理构造演化。来自捕获光谱和核磁共振的丰富信息为淡层水环境中低电阻率对比砂岩的流体分型提供了巨大的应用。非常规油藏的岩性识别以及其他油藏特性表征。解释指导了候选测试的选择,并已得到测试结果的证实。第一个形成是碎屑层序,其中流体类型是主要挑战。在常规原木上,就电阻率读数,缺乏密度-中子穿越等而言,大多数沙子具有相似的岩石物理特征。此外,源自伽玛射线和新鲜地层水的可疑粘土体积使解释更具挑战性鉴于这些困难,公司决定购买捕获光谱仪和NMR测井仪,以便对该结构的第一口勘探井得出可靠的结论。清楚地确定了所有含烃区。光谱-核磁共振结合清楚地揭示了主要含气砂的沉积序列。对于另一个区域,与传统的GR估计相比,光谱测井显示的粘土体积要低得多,并且即使没有密度-中子交叉,密度-NMR组合也显示该区域是含气的。在块状含水砂的顶部发现了一个气顶,人们期望在同一块砂的结构中可以发现更多的气体。在同一口井的底部,发现了一个放射性很强的块状地层,即天然伽马。射线光谱法显示or和钾的读数都很高;中子和密度测井仪也不能提供确定的岩性和孔隙度。捕获光谱法确定了地层顶部的一种干净的沙子。 NMR的渗透率也很高。 T2的很长的弛豫时间表明存在非常轻的油的潜力很大。rn从伽玛射线捕获光谱和NMR的综合测量得出的详细矿物学信息表明,该地层的沉积环境很可能是冲积沉积,而源岩为风化花岗岩。这个基于对数的结论有助于校准现有的储层模型。

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